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Dendritic, trellis, and radial drainage patterns are common in geology, each indicating different underlying geological features and structures.
A dendritic drainage pattern is the most common form in which the tributaries resemble the branching pattern of tree roots, developing in areas with uniform underlying geology. In contrast, a trellis drainage pattern is seen in folded terrains like the Appalachian Mountains, while a radial drainage pattern flows outward from a central elevated point, common around features like volcanoes.
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